Mushroom clouds consist of a head and a stem, formed by a convective updraft driven by the rapid expansion and cooling of superheated matter in explosions.
The size of a mushroom cloud depends on the yield of the explosion, with nuclear mushroom clouds being larger than those from conventional explosions.
Condensation rings can form behind the shock wave of a mushroom cloud, resulting in visible rings of expanding vapor.
Mushroom clouds produced by nuclear explosions have yet to break through the tropopause and reach the heights of cumulonimbus clouds.
The largest nuclear bomb detonated was the Mark 18, with a yield equivalent to 540 kilotons of TNT.